## Abstract We develop a new method for analysis of meandering channels based on planform sinuosity. This analysis objectively identifies three channelβreach lengths based on sinuosity measured at those lengths: the length of typical, simple bends; the length of long, often compound bends; and the
Types of river channel patterns and their natural controls
β Scribed by Alabyan, Andrei M.; Chalov, Roman S.
- Publisher
- John Wiley and Sons
- Year
- 1998
- Tongue
- English
- Weight
- 204 KB
- Volume
- 23
- Category
- Article
- ISSN
- 0360-1269
No coin nor oath required. For personal study only.
β¦ Synopsis
River channel patterns are thought to form a morphological continuum. This continuum is two-dimensional, defined by plan features of which there are three (straight, meandering, branching), and structural levels of fluvial relief of which there are also three (floodplain, flood channel, low-water channel). Combinations of these three categories define the diversity of patterns. One of the most important factors in channel development is stream power, defined by water discharge and river slope. The greater the stream power, the stronger the branching tendency, but threshold values of stream power are different for the three different hierarchical levels of channel relief. The critical stream power values and hydrological regime together define the channel pattern, and analysis of the pattern type can be undertaken using effective discharge curves.
π SIMILAR VOLUMES
## Abstract Nitrogen (N) and phosphorus (P) dynamics in the Kuparuk River in arctic Alaska were characterized in a 3βyear study using routine samples near the mouth of the river at the Arctic Ocean, synoptic wholeβriver surveys, and temporally intense sampling during storms in three headwater basin
## Abstract Temporal stability of soil moisture spatial patterns has important implications for optimal soil and water management and effective field monitoring. The aim of this study was to investigate the temporal stability of soil moisture spatial patterns over four plots of 105 m Γ 135 m in gri